What are the big ignited provinces?

The large igneous province (RT) is a large part of the Earth's surface covered with a magmatic (ie igneous) rock, usually basalt, but also a rhyolite that exploded in a geologically short period of time, usually a million years. The large igneous province can be hundreds of meters thick, usually covered with millions of square kilometers in the range, for a total volume of about a million cubic kilometers. Most large igneous provinces are produced by a volcano complex relaxing about a cubic kilometer of lava per year (a lot) for at least a million years, although a sudden super-erup can sudden land responsible for creating new land (continuous breast). Two examples include Central America created through volcanic activity as well as the Caribbean Islands. The whole area around Indonesia is vulcanically active, and most of its islands are cooled magma rather Normal Cratons. Originally, all continents were created by volcanic action, but most of them are so old that evidence of specificIt is difficult to come to the large igneous provinces in the ancestor's times. The ancient large ignited provinces can consist of swarm of players, which means that they store rock veins that suddenly cut over other rock layers and perform on geologists.

Large igneous provinces can also be responsible for most of the historical bulk demise. Unlike the great asteroid impacts, large igneous provinces are determined with a certain regularity and their duration over a million years suffers from a permanent burden on animal species. Events laid down by a large igneous province are called "flood basalt" or "flood basalt events" when they occur on the ground. The event of flood basalt, which produced deccan traps in India, is considered to be the main contributor to the end-Permian mass extinction, sometimes called a "great dying" that killed 95% of all types of land and sea on Earth.

Large igneous provinces can now be found in Ethiopia, northwest United States, Brazil, Uruguay, South Africa, Antarctica, Russia and China. Some large igneous provinces cover parts of continents that are separated today but were connected in the distant past. One example is a large igneous province that includes part of South Africa and Antarctica. Both were once part of the Gondwan continent.